• 대한기계학회논문집B
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• 제30권12호
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• pp.1211-1217
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• 2006

This study is focused on oxidation prevention of STS430, which is generally used as solid oxide fuel cell(SOFC) interconnect at intermediate operating temperatures with oxidation-proof coatings. Inconel, $La_{0.6}Sr_{0.4}CoO_3(LSCo)$ and $La_{0.6}Sr_{0.4}CoO_3(LSCr)$ were chosen as coating materials. Using a radio frequency magnetron sputtering method, each target material was deposited as thin film on STS430 and was analyzed to find out favorable conditions. In this study, LSCr-coated STS430 can reduce electrical resistance to 1/3 level, compared with uncoated STS430. Also, long-term durability test at $700^{\circ}C$ for 1000 hours tells that LSCr thin layer performs an important role to prohibit serious degradations. Superior oxidation-resistant characteristic of LSCr-coated STS430 is attributed to the inhibition of spinel structure formation such as $MnCr_2O_4$.

• 자원환경지질
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• 제25권1호
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• pp.27-39
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• 1992

Several pyrophyllite deposits occur around the Milyang area where Cretaceous andesitic rocks and spatially related granitic rocks are widely distributed. Pyrophyllite ores consist mainly of pyrophyllite, and quartz with small amount of sericite, pyrite, dumortierite, and diaspore. The andesitic rocks and spatially related granitic rocks in this area suggest that they could be formed from the same series of a calc-alkaline magma series. The contents of $SiO_2$, $Al_2O_3$, LOI(loss on ignition) are enriched, and $K_2O$, $Na_2O$, CaO, MgO, $Fe_2O_3$ are depleted in altered andesitic rocks and ores. Enrichment of As, Cr, Sr, V, Sb and depletion of Ba, Cs, Ni, Rb, U, Y, Co, Sc, Zn are characteristic during mineralization. The pyrophyllite ores can be discriminated from the altered-and unaltered wall-rocks by an increasing of $(La/Lu)_{cn}$ from 4.18~22.13 to 8.98~55.05. In R-mode cluster analysis, Yb-Lu-Y, La-Ce-Hf-Th-U-Zr, $TiO_2-V-Al_2O_3$, Sm-Eu, $CaO-Na_2O-MnO$, Cu-Zn-Ag, $K_2O-Rb$ are closely correlated. In the discriminant analysis of multi-element data, $P_2O_5$, As, Cr and $Fe_2O_3$, Sr are helpful to identify the ores from the unaltered-and altered wall-rocks. In the factor analysis, the factors of alteration of andesitic rocks and ore mineralization were extracted. In the change of ions per unit volume, $SiO_2$, $Al^{3+}$ and LOI are enriched and $Na^+$, $K^+$, $Ca^{2+}$, $Mg^{2+}$, $Mn^{2+}$ and $Fe^{3+}$ are depleted during the alteration processes. The Milyang and the Sungjin pyrophyllite deposits could be mineralized by hydrothermal alteration in a geochemical condition of low activity ratio of alkaline ions to hydrogen ion with reference to spatially related granitic rocks.

• 한국지구과학회지
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• 제34권4호
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• pp.313-328
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• 2013

영남육괴 북동부에 분포하는 쥐라기 심성암체들은 유라시아대륙의 동북부지역 아래로 고태평양판의 섭입에 의해서 야기된 활발했던 화성활동의 산물이다. 지화학적 연구를 통하여 이 지역에 분포하는 화강암류의 성인과 지구조환경을 유추하여 보았다. 영남육괴 북동부에 위치하는 울진화강암류는 비알칼리(subalkaline)영역에 속하는 칼크-알칼리(calc-alkaline)계열로, 분화에 따른 주성분원소의 변화 경향은 전반적으로 다른 지역의 쥐라기 화강암류의 분화 경향과 유사하게 나타나지만, 각 암체의 분화경향이나 화학조성을 살펴볼 때 각 암체의 마그마 근원물질은 서로 다른 것으로 사료된다. 울진화강암류는 연구지역 주변에 분포하는 다른 화강암류와 비교하여 $Al_2O_3$의 함량 및 Cr, Co, Ni, Sr, Y, Nb 등 미량원소의 함량에서 뚜렷한 차이를 보인다. 울진화강암류의 지화학적 특징은 높은 $Al_2O_3$, Sr 함량과 높은 Sr/Y, La/Yb비를 가지며, 낮은 Y과 Yb함량과 같은 슬랩용융(slab-melting)으로 생성된 아다카이트에서 흔히 관찰되는 지화학적 특성을 나타낸다. 울진화강암류의 주성분원소($SiO_2$, $Al_2O_3$, MgO) 및 미량원소(Sr, Y, La, Yb) 함량 범위는 아다카이트질 화강암의 범주에 포함되며, 지화학적 특성, 지구조환경 및 관입시기가 일본의 북서부 Hida belt에 위치한 Yatsuo심성암체와 유사하다. 연구지역의 암석의 희토류원소 패턴은 경희토류가 중희토류에 비해 부화($(La/Yb)_{CN}=10.6-103.4$)되어 나타나며, Eu의 부(-)이상을 보이지 않는다. ANK vs. A/CNK과 지구조판별도에서 화강암류의 모마그마는 I-type의 화산호 화강암의 특성을 나타내며, 이자나기(Izanagi)판의 섭입에 의한 압축장 응력이 작용하는 대륙연변부에서 생성된 것으로 해석된다.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2002년도 하계학술대회 논문집 Vol.3 No.2
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• pp.629-633
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• 2002

The degradation behaviour of ZPCCL-based varistor ceramics composed of 97.5 mol%ZnO-0.5 mol% $Pr_6O_{11}-1.0$ mol% $Cr_2O_3-0.5$ mol% $La_2O_3$ was investigated under various DC accelerated aging streses. The varistor ceramics sintered for 1 h exhibited excellent nonlinearity, in which the nonlinear exponent is 81.6 and the leakage current is $0.2{\mu}A$. It was found that this varistor ceramics possess high stability, in which the variation rates of varistor voltage, nonlinear exponent, and leakage current are -1.14%, -3.7%, and 85.0%, respectively, against DC accelerated aging stress. On the contrary, the varistor ceramics sintered for 2 h also exhibited high nonlinearity and stability, but they were bad characteristics, compared with the varistor ceramics sintered for 1 h.

• 수산해양교육연구
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• 제19권1호
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• pp.1-7
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• 2007

The purpose of this study was to investigate geochemical characteristics of surface sediments in the Keum river estuary adjacent to coastal area. For this study we collected the 21 surface sediments samples. Mean size of surface samples was $3.24{\sim}6.65{\phi}$ on inner estuary and was $2.15{\sim}3.42{\phi}$ on outside estuary. Surface samples were composed of silt on inner estuary and were composed of sand which was more larger than $4{\phi}$ on outside estuary. Most major elements except CaO, $Na_2O$ showed good relationships between variation of contents and grain size. Contents of $Al_2O_3$, $Fe_2O_3$, MgO, $K_2O$, $TiO_2$, $P_2O_5$ and $M_nO$ were increased predominately owing to the variation of mean size of surface samples. Contents of Co, Cr, Cu, Li, Sr, Zn, La, Ce, Pb, Rb, Nd have a good relationships with grain size but Ba, Th, Sm have not. All of major and minor elements contents except $K_2O$ and Ba were less than world mean contents of shallow surface sediments but apprehend a high pollution possibility on silt sediments in the estuaries.

• 자원환경지질
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• 제26권3호
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• pp.337-347
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• 1993

Mineralogical and geochemical studies on some pyrophyllite deposits in Milyang area, Kyeongnam Province (Milyang and Sungjin mine) were carried out in order to investigate dispersion patterns of chemical elements in altered volcanic wallrocks, and to interpret genetic environments of the pyrophyllite deposits. Cretaceous andesitic and tuffaceous rocks, and pyrophyllite ore specimens were collected from the dumps and drilling cores. Andesitic wallrocks were grouped as unaltered and altered rocks in the order of pyrophyllitization. Vertical dispersion patterns and relative mobilities of chemical elements in volcanic wallrocks were discussed. Geochemical environment in the Milyang area is characterized by the occurrence of boron minerals such as dumortierite coexisting with pyrophyllite ores, and tourmaline in granitic rocks. Unaltered andesitic rocks are mainly composed of plagioclase, pyroxene and hornblende, and were propylitized and saussuritized. Altered andesitic rocks are bleached and consist of quartz, sericite, pyrophyllite, kaolinite, chlorite and disseminated pyrite. Pyrophyllite ores are mainly composed of quartz, pyrophyllite, dumortierite, dissemianted pyrite and some diaspore. Enrichment of $SiO_2$, $Al_2O_3$, LOI (loss on ignition), As and Cr, and depletion of $K_2O$, $Na_2O$, CaO, MgO and total Fe are characteristic during alteration process. The REE patterns show that the pyrophyllite deposits could be originated from the continental margin volcanics. The $(La/Lu)_{cn}$ ratios of the pyrophyllite ores increase from 4.2~23.2 to 2.67~128.8 owing to strong acidic hydrothermal alteration. Vertical dispersion patterns of $Al_2O_3$, $K_2O$, $Na_2O$, CaO, MgO, $Fe_2O_3$ (total Fe), As, Au, Sb, Cr and Sr in the wallrocks show the location of orebodies. Particularly dispersion patterns of $Al_2O_3$ and Cr indicate the extension of orebodies. Anomalous distribution of Au, As and Sb in wallrocks shows potential for gold occurrence below the pyrophyllite deposits. Judging from the relative mobilities of elements in wallrocks, $Al_2O_3$ could be added from hydrothermal solution, and the silicified rone be formed from the excess of $SiO_2$.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2011년도 추계학술대회 초록집
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• pp.91.2-91.2
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• 2011

고체산화물 연료전지의 연결재의 필요한 물성으로는 공기극과 연료극을 차폐시켜줄 수 있는 고밀도와 구성 소재간의 전기적으로 연결될 수 있는 전기전도도 및 낮은 이온전도도. 산화극과 환원극에서 화학적 안정성과 타 구성 소재와의 열팽창 계수가 일치 등이 중요한 특성으로 필요하게 된다. 이를 위해 LaCrO3계 연결재가 주로 사용되어 왔다. 그러나 LCO계 연결제는 $1400^{\circ}C$ 이상의 높은 소결 온도와 이로 인한 Cr의 휘발로 인한 타 구성소재와의 반응 등으로 인해 저온소결의 필요성이 재기되고 있는 소재 이다. 본 연구에서는 LCO계 구성 소제에 소결 조제를 첨가하여 저온에서 결정성 및 소결거동, 전기적 특성을 평가하였다.

• 대한환경공학회지
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• 제27권6호
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• pp.651-656
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• 2005

톨루엔은 섬유산업 공정에서 발생하는 주요한 유해성 대기 오염원으로 간주된다. 본 연구에서는 ${\gamma}-Al_2O_3$를 지지체로 한 전이 금속 산화물 촉매(Cu, Mn, V, Cr, Co, Ni, Ce, Sn, Fe, Sr, Cs, Mo, La, W, Zn)를 제조하여 톨루엔 완전 산화 반응을 조사하였다. XRD, FE-SEM, BET와 TPR 기법을 사용하여 금속 촉매의 특성을 조사하였다. 촉매 가운데 Cu/${\gamma}-Al_2O_3$ 촉매가 가장 우수한 활성을 보여주었다. BET결과 촉매 활성의 증가는 비표면적과는 관련이 적은 것으로 나타났으며, X선 회절 분석에서 대부분의 촉매들이 무정형으로 존재함이 관찰되었다. FE-SEM을 관찰한 결과, 전이금속 산화물 촉매 중 구리산화물 촉매가 지지체 표면에 고르게 분산되어 있음을 확인할 수 있었다. 톨루엔 산화반응에 따른 촉매활성 효과는 ${\gamma}-Al_2O_3$ 지지체 위에 전이금속 산화물 촉매가 고르게 분산된 점과 촉매 표면의 우수한 환원 특성에 기인하는 것으로 설명할 수 있었다.

• Korean Chemical Engineering Research
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• 제48권2호
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• pp.172-177
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• 2010

본 논문에서는 SOFC 금속연결재로서 Crofer22APU를 적용하고자 표면에 전도성 산화막($La_{0.8}Sr_{0.2}CoO_3$)을 습식코팅 후, SOFC 작동환경에서 산화거동, 전기적 특성변화 및 미세구조 변화를 관찰하였다. 코팅 전 샌드블러스트 장치를 이용한 Crofer22APU 표면처리를 통하여 코팅막/금속의 접합특성을 개선시킬 수 있었으며, 320 mesh의 입자크기를 갖는 알루미나 분말을 이용하여 표면처리한 경우 접착특성이 극대화되었다.$La_{0.8}Sr_{0.2}CoO_3$ 코팅된 시편의 전기적 특성 평가는 4-wire 법을 이용하여 SOFC 작동환경에서 약 4,000 시간 장기성능 평가하였으며 $12mW{\cdot}cm^2$의 낮은 면저항값을 얻을 수 있었다. 실험종료 후 미세구조 분석결과에서도 전도성 산화막($La_{0.8}Sr_{0.2}CoO_3$) 코팅이 금속의 부식으로 인한 산화층의 생성속도를 늦추고 이로 인한 금속의 전기적 특성이 감소하는 것을 방지하는데 유효함을 확인하였다.

• 자원환경지질
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• 제56권6호
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• pp.745-764
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• 2023

In the Republic of Congo, Banded iron formations (BIFs) occur in two areas: the Chaillu Massif and the Ivindo Basement Complex, which are segments of the Archean Congo craton outcropping in the northwestern and southwestern parts of the country. They show interesting potential with significant mineral resources reaching 2 Bt and grades up to 60% Fe. BIFs consist mostly of oxide-rich facies (hematite/magnetite), but carbonate-rich facies are also highlighted. They are found across the country within the similar geological sequences composed of amphibolites, gneisses and greenschists. The Post-Archean Australian Shale (PAAS)-normalized patterns of BIFs show enrichment in elements such as SiO₂, Fe₂O₃, CaO, P₂O₅, Cr, Cu, Zn, Nb, Hf, U and depletion in TiO₂, Al₂O₃, MgO, Na₂O, K₂O, Sc, Th, Ba, Zr, Rb, Ni, V. REE diagrams show slight light REEs (rare earth elements; LREEs) compared to heavy REEs (HREEs), and positive La and Eu anomalies. The lithological associations, as well as the very high (Eu/Eu^*)_SN ratios> 1.8 shown by the BIFs, suggest that they are related to Algoma-type BIFs. The positive correlations between Zr and TiO₂, Al₂O₃, Hf suggest that the contamination comes mainly from felsic rocks, while the absence of correlations between MgO and Cr, Ni argues for negligeable contributions from mafic sources. Pr/Pr^* vs. Ce/Ce^* diagram indicates that the Congolese BIFs were formed in basins with redox heterogeneity, which varies from suboxic to anoxic and from oxic to anoxic conditions. They were formed through hydrothermal vents in the seawater, with relatively low proportions of detrital inputs derived from igneous sources through continental weathering. Some Congolese BIFs show high contents in Cr, Ni and Cu, which suggest that iron (Fe) and silicon (Si) have been leached through hydrothermal processes associated with submarine volcanism. We discussed their tectonic setting and depositional environment and proposed that they were deposited in extensional back-arc basins, which also recorded hydrothermal vent fluids.